AOS midterm Flashcards
define: concentration
number of molecules of a substance per unit volume
C = N/V
the amount of pollutant in a given volume of air
how much stuff is mixed in some mixture of many materials
convert 0 C to Kelvin
273K
convert -273 C to K
0 K
units of the SI system
m, kg, s, K/C
what is the current meter standard?
distance traveled by light in a vacuum in a known fraction of a second
what is the density of water?
1 kg/L
how does the atomic clock time standard work?
the oscillation period between two ground state levels in a cesium atom
what is mixing ratio?
ratio between the amount of the pollutant vs the amount of other gasses
(amount of one substance) / (amount of all the other substances)
what are the concentration units for gasses?
molecules per unit volume (mol./cm3)
what are the concentration units for particles?
mass per unit volume (micrograms/cm3)
effect of a change in volume on mixing ratio
no change; just spreading the particles out, not changing the numbers of particles
effect of a change in volume on concentration
concentration depends on volume
increase in V, decrease in C
decrease in V, increase in C
what is the steady-state-box model?
representation of environment as a ‘box’ and measuring inflow and outflow based on that volume
it is in ‘steady state’ when the concentration (and total amount) is not changing
what is a ‘source?’
everything that introduces pollutants into the air in the box
e.g. direct emission (by cars); transport by wind; chemical transformation; re-suspension (pollutant becoming free from liquid or or solid surface and become airborne)
what is a ‘sink?’
processes that remove or convert pollutants
e.g. ventilation (wind blows them away); chemical conversion; deposition (pollutant deposited to ground)
what is a ‘rate?’
quantification of how fast something is happening
rate of emission/loss (S/L)
S/L = (amount emitted or lost in time interval t) / (time interval t)
how to calculate the amount of material in the volume of space
source rate - sink rate = S - L
box model equation (steady state concentration of pollutant), q
q = (S or L)*tau / V
what percentage of earth’s surface is water?
70%
where did life first develop and why?
the oceans because the water protected from harmful UV rays
how did the earliest life forms get their energy?
they were heterotrophic - used organic molecules and broke them down to harvest the energy (fermentation)
why didn’t heterotrophy last?
these organic compounds were not abundant enough and supplies ran low quickly
what solved the organic carbon scarcity problem?
autotrophy - harvesting energy from inorganic substances in their environment
what is photosynthesis?
an autotrophic process that permitted the organisms to harvest energy from the sun - oxygenic and anoxygenic
what was the early type of photosynthesis?
anoxygenic - produced organic matter but did not produce molecular oxygen as a byproduct; used sulfur compounds
what was the most important evolutionary step and why?
evolution of oxygenic photosynthesis
oxygen started to accumulate in the environment
oxidized substances in the Earth’s crust
oxygenated the oceans
accumulated in the atmosphere, and absorbed the shortest wavelengths of solar ultraviolet radiation
led to formation of ozone gas from the oxygen
formation of the ozone layer and the Earth’s stratosphere
aided the absorption of solar UV radiation and eventually allowed life to evolve on dry land, outside of the oceans
changes to the Earth environment from this oxygenation due to photosynthesis
removes CO2 and adds O2; atmospheric CO2 decreases over time –> long, slow, cooling of the earth; too much oxygen for current anaerobic organisms, so they die off; ozone layer forms, allowing more diverse life forms to develop
how does ozone absorb UV radiation?
O3 + hv –> O2 + O
where hv is the energy of a photon of light
how is ozone formed?
illuminating oxygen w UV radiation
O2 + hv –> O + O
O + O2 + M –> O3 + M
what is the largest mass extinction ever and how much of the population was lost?
Permian Triassic mass extinction (PT event); loss of 60% of species
how did early humans impact the environment?
agriculture (cultivation of land, burning of wood, animal waste), heating (open wood fires indoors and burning of coal), and manufacturing (copper/bronze metals and leather tanning) altered the landscape and/or polluted the air with combustion of organic materials
what was the environmental impact of deforestation?
reduces a local sink for carbon dioxide
difference between pre-industrial society’s impacts on the environment and today’s impacts
pre: impacts were locally restricted; total world population was small; energy use was limited because it was based on renewable energy
calculate total pollution produced
C x r x Ap
C = population size [persons]
r = per capita resource consumption [resource units/person]
ap = pollution per resource unit consumed [pollt. units/res.units]
IPCC scenarios of population growth criteria
globalization vs local development (1 vs 2)
economic vs environmental emphasis (A vs B)
IPCC A1 marker scenario
globalization with economic emphasis –> rapid convergent growth (second smallest future population)
IPCC A2 marker scenario
local development with economic emphasis –> fragmented world (largest future population)
IPCC B1 marker scenario
globalization with environmental emphasis –> convergence with global environmental emphasis (smallest future population)
IPCC B2 marker scenario
local development with environmental emphasis –> local sustainability (second largest future population)
what drives the rise in atmospheric CO2
the burning of fossil fuels mainly with contributions from deforestation and other types of land use change
define weather
state of the atmosphere as we experience it instantaneously
define climate
average weather over an extended period of time in a specific region
define global climate
globally averaged weather over an extended period of time
define global average temperature
stable parameter for climate
how can we study past climates?
ice cores - snow layers with chemical indicators of past climates
how quickly can the climate change?
as quickly as 10 years
what is firn?
snow over 1 year old
what is a hoar layer?
a weak layer of frost that forms on the snow during calm, clear, and humid conditions
how deep do you have to go to get ice cores?
2m+
what do ice records tell us about past climates?
CO2 mixing ratios
relative temperature by the ratio of hydrogen and deuterium
strong covariance of atmospheric CO2 and temperature
what are earth’s permanent gasses and at what percent?
nitrogen (78%), oxygen (20%), argon (1%), and trace gasses
what are earth’s variable gasses?
water vapor (1) and carbon dioxide (2)
layers of the atmopshere (ground up)
troposphere, stratosphere, ozone layer, mesosphere, ionosphere (aurora)
what is the kind of rate of change of pressure with altitude?
exponential
how do pressure and density and altitude mathematically relate?
pressure and density both decrease by a half for every 5.5 km increase in altitude
what is boyle’s law
P1V1 = P2V2 (inverse relationship)
what is adiabatic expansion?
lower parcel temperature as parcel rises in atmosphere and expands
how much does the greenhouse effect raise overall temp by?
33K
what is thermal energy?
how hot a body is; more the hotter it is (higher temp)
what is radiative energy?
light carries energy
what is chemical energy?
molecules can store energy
what is the suns surface called?
the photosphere
what is the temperature at the photosphere?
~6000K
how does the sun generate energy?
nuclear fusion 2H —> He + (thermal) energy
what is a black body?
a perfect blackbody absorbs all wavelengths of electromagnetic radiation (emr) that fall on it
what is kirchoff’s law?
a blackbody also emits all wavelengths of emr
what happens to a blackbody at a lower temp and example
less radiation is emitted and color becomes redder
incandescent lamps behave like black bodies
what happens to a blackbody at a higher temp
peaks at shorter wavelengths and more energy is emitted overall
what is albedo
percentage radiation reflected on earth
what is the average surface temp of earth without an atmosphere
255K
what happens to the radiation that reaches earth
UV absorbed by O2 and O3; IR is absorbed by CO2 and H2O except for a small atmospheric window that lets some of earths IR out; most visible light is not absorbed
what is the greenhouse effect?
upgoing IR is absorbed and emitted back to the ground thus heating the earth more with the radiation
how much of earth’s surface is covered in clouds?
about half at any given time
name 2 types of clouds
cumulus and cirrus
effect of high clouds on earth;s albedo
high clouds have a low albedo so do not affect solar radiation in a major way
greenhouse effect => weak
oevrall warming
effect of low clouds on earth’s albedo
high albedo of low clouds significantly reduce solar radiation reaching earth’s surface
greenhouse effect => warming not as strong as cooling effect from albedo
overall planetary cooling
what is the influence of aerosols/haze on the atmosphere?
similar to cooling by clouds
increases albedo —> cooling effect
signs of climate change
temperature change
change in cloudiness and rainfall
changes of arctic sea ice, ice caps, and glaciers
variation of sea level
climate change from natural causes
sunspot cycles; milankovitch cycles; volcanic eruptions
how do sunspot cycles effect climate change?
the suns emissions vary slightly in an 11 year period but the intensity is too weak to actually be noticed
how do milankovitch cycles affect climate change?
variations in earth’s orbit with periods of 22000 41000 and 100 000 yrs and could have been triggers for ice ages but magnitude is too small to explain current changes
how do volcanoes affect climate change?
ash and other particles block sunlight (albedo) => surface cools down
greenhouse gasses and primary sources
water vapor (no main source), CO2 (fossil fuel combustion), methane food production – rice and cows), N2O (agricultural - fertilized - soils), CFCs (refrigerants and industry)
How can aerosol (haze) impact the climate?
White aerosol can lead to cooling of the surface
Black aerosol can warm the atmosphere
how do we know climate change is real?
average land-surface air temp rose 1.3C; sea level has risen over the past 200 yrs; global glacier retreat; arctic sea ice retreat
best and worst scenarios for future climate change
best: we actively and effectively reduce emissions, temp will increase 1 degree celcius by the end of the century and then slowly decrease
worst: little reduction in greenhouse emissions, temp will increase 4 C by 2100 and 8 C by 2300
what is negative feedback
cause –> effect –> suppress
the effect suppresses the cause, decreasing the effect
positive feedback
increases the effect - self-sustaining
what is geoengineering and what are the 2 methods
manipulation of the earth’s climate system to counteract the effects of climate change caused by greenhosue gas emissions [last resort]
eg.
remove atmospheric carbon dioxide or reduce emissions via carbon sequestration (CDR)
manage solar radiation reaching earth’s surface (SRM)
alternative sources of energy
geothermal energy hydroelectric power nuclear energy biofuels wind energy solar radiation photovoltaics (solar cells)
what is CDR
carbon dioxide removal (cdr) - remove CO2 from atmosphere and store underground
what is srm
solar radiation management (srm) - reduce sunlight reaching earth’s surface
methods of CDR
reforestation, biochar, enhancement of natural weathering processes, enhancement of oceanic uptake of CO2, direct engineered capture of CO2,
methods of srm
increase surface reflectivity,
when was the ozone hole discovered?
1986
where can most ozone be found?
stratosphere
difference between good ozone and bad ozone
good is in stratosphere bad is below and considered smog
what is the chapman cycle
the conversion of oxygen to ozone and back again
chemical mechanism for the source of ozone in the chapman cycle
O2 + hv —> O + O
2x O + O2 —> O3
net: 3O2 —> 2O3
chemical mechanism for the sink of ozone in the chapman cycle – photolysis
O3 + hv —> O2 + O
O + O3 —> O2 + O2
net: 2 O3 —> 3O2
catalytic chemical mechanism for ozone destruction
O3 + X —> XO + O2
XO + O3 —> X + 2O2
net: 2O3 —> 3O2
natural catalysts for ozone destruction
NO, OH, Cl, Br
what is a vertical ozone column (TOC)
all the ozone in the column of 1 cm2 cross-section from the ground to space
classes of UV radiation and effects
A - lowest energy, not absorbed by ozone, doesn’t cause sunburn but can contribute to skin cancer; B - most absorbed by ozone layer, can cause sunburn and skin cancers; and C - most energetic, hazardous, used for sterilization, but is completely absorbed by the ozone layer
types of skin cancers
basal cell carcinomas; squanous cell carcinomas; melanoma
what are CFCs chemically
organic molecules where the H atoms have been completely replaced by F and Cl (completely artificial); very unreactive and chemicall stable and not harmful to humans, so seem like a good idea for aerosols but because they are unreactive, nothing removes them
timeline of the ozone hole over antarctica
May: sunset cooling; June: polar vortex; aug/sept/oct: sunrise, ozone hole develops; Nov.: polar vortex break-up
ozone hole appears in august
ozone hole max in september
ozone hole starts to fade in late october/early november
what is the polar vortex and some effects
wind circulation around antarctica in the stratosphere
inhibits air exchange with lower latitudes (air is trapped)
air in vortex cools down by thermal radiation
ozone depleted air can not be replensished
what are polar stratospheric clouds - PSCs
clouds of ice particles in 15-25 km altitude
what are psc types 1s made of
frozen nitric acid on a sulfuric acid core
what are psc type 2s made of
ice frozen onto nitric acid cores (frozen onto PSC type 1s)
what do pscs do to the air chemistry
convert reservoir to active species by heterogeneous reactions and removal of NO2
what is the molina cycle
a catalytic ozone destruction cycle with Cl as the catalyst that becomes important only with high levels of chlorine